Porphyritic textures suggest a complex cooling and crystallization history. one that includes at least two rates of crystallization.
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Q9: The magmas formed beneath spreading ridges are
Q10: Magma composition may change by crystal settling.
Q11: Partial melting explains the origin and composition
Q12: Magmas formed at subduction zones are mostly
Q13: Phaneritic textures indicate that the rock formed
Q15: Volcanoes always erupt magmas of the same
Q16: Pegmatites are composed of very large crystals
Q17: Rhyolite forms when a mafic magma cools
Q18: Dikes are concordant and sills are discordant.
Q19: Laccoliths are more similar to sills than
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